Geomorphology Flashcards
The structure of the Earth
4 layers
MOLTEN: Liquid
MAGMA: molten
MANTLE: The layer of molten material around the earth’s core
CRUST: the outer layer of the earth , formed of solid rock
PROCESSES THAT CHANGE ROCKS IN THE ROCK CYCLE
Pressure and temperature turn sedimentary rocks into igneous rocks
Pressure and temperature turn igneous rocks into metamorphic rocks
Temperature turns sedimentary rocks into metamorphic rocks
Weathering turns metamorphic rocks into sedimentary rocks
Igneous Rocks
magma rises through the crust, cools and crytallises into new rock
intrusive igneous activity
occurs when the magma intrudes into spaces underground and hardens
intrusive landforms
- Batholith
- Laccolith
- Lopolith
- Dyke
- Sill
- Pipe
Plate tectonic
a section of the Earth’s crust which can move on the mantle
Plate boundary
the edge of the tectonic plate
Continental drift
Continental drift
Pangea split into
Laurasia (the northern continent) and
Gondwana (the southern continent).
evidence supporting continental drift
- similar fossils found in different continents
- rock formations
- similar coal deposits
- continents are like a puzzel and fit into each other
formaton of folds
- form when tectonic plates push together, placng the rock under great pressure
- the rock layers compress and form fold features
fold mountains are normally formed on
the edges of collding plates
Types of folds
- overthrust fold
- recmbent fold
- overfold
- monocline
- syncline
- antcline
overthrust fold
- also called a nappe
- pressure is very great
- fold breaks
- one limb pushed forward the other
recumbent fold
- occurs under extreme pressure
- limb becomes nearly horizontal
overfold
- one limb is more steeply inclined than the other
monocline
- simplest fold
- step-like fold strata
syncline
- where rock layers fold downwards in a ‘U’shape
anticline
- where rock layers fold upward in a ‘n’ shape
effects of mountains on people
- terrace farming
- eco-tourism
- hydroelectric power
faulting
line of weakness in the rock or strata
causes of faults
- rocks crack due to pressure
- one section of rock may slide alongside or over another
- lateral or vertical movement
- tension
types of faults and landforms
- normal fault
- reverse fault
- lateral tearing fault
normal fault
causes
caused by tension